Geology and land use as key drivers for hydrogeochemistry in a mining district of the Quadrilátero Ferrífero, Brazil: implications for water management strategies
Gabriel Negreiros Salomão, Normara Yane Mar da Costa Andrade, Gabriel Soares de Almeida, Rafael Tarantino Amarante, Roberto Dall’Agnol, Paulo Rógenes Monteiro Pontes, Prafulla Kumar Sahoo, Lucas Pereira Leão, Eduardo Duarte Marques, Emmanoel Vieira da Silva-Filho

TL;DR
This study explores how geology and land use affect water chemistry in a Brazilian mining area, offering insights for better water management.
Contribution
The study introduces reference values for Fe and Mn using the UTL method, tailored to local geochemical conditions in a mining district.
Findings
Mixed bicarbonate facies dominate in metavolcano-sedimentary terrains, while granitoids show alkali enrichment.
Urban areas increase Na, Cl, sulfate, and nutrients in water.
Fe and Mn levels rise during the rainy season in mining and urbanized areas.
Abstract
This study investigated the hydrogeochemical characteristics of surface waters in the Congonhas Mineral District (CMD), located in the southern portion of Quadrilátero Ferrífero, Brazil. A total of 38 sites were monitored between 2021 and 2024 to understand seasonal and spatial variability across distinct lithologies and land uses. Hydrogeochemical patterns revealed dominant mixed bicarbonate facies associated with metavolcano-sedimentary terrains, while domains of granitoids exhibited alkali enrichment. Waters under the influence of larger Urban settlements were enriched in Na, Cl, sulfate, and nutrients. By integrating geospatial classification, seasonal sampling, and robust statistical techniques, we investigated the behavior of Fe and Mn, key elements influenced by both natural geological sources and mining activities. Reference values for geochemical background and baseline…
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Taxonomy
TopicsMine drainage and remediation techniques · Geochemistry and Geologic Mapping · Tailings Management and Properties
